ارزیابی توانمندی های ژئوتوریستی مناطق کارستی جنوب غرب استان لرستان (مقاله علمی وزارت علوم)
درجه علمی: نشریه علمی (وزارت علوم)
آرشیو
چکیده
منطقه جنوب غربی لرستان در پهنه ناهمواری زاگرس چین خورده واقع شده است و بخش زیادی از واحدهای سنگ شناسی این محدوده مطالعاتی دارای ساختار آهکی و انحلال پذیر است. به همین دلیل ژئومورفوسایت های کارستی متنوعی در جنوب غربی لرستان در دو حوضه آبریز کشکان (شهرستان های پلدختر و معمولان) و حوضه آبریز سیمره (شهرستان های کوهدشت و رومشکان) شکل گرفته است که تعداد زیادی از آنها می توانند مقصدهای گردشگری قلمداد شوند. هدف این پژوهش ارزیابی توانمندی های ژئوتوریستی سازندهای کارستیک در جنوب غربی استان لرستان با پیمایش و تحلیل نقشه ها و روابط فضایی آن ها با قلمروهای کارستی از طریق مدل کوبالیکوا و کیرچنر (2016) است. برای اجرای مدل، جامعه آماری پژوهش شامل 8 نفر از کارشناسان سازمان میراث فرهنگی و 7 نفر از اساتید دانشگاه لرستان می باشد. بر اساس نتایج بدست آمده به ترتیب سه سازند آسماری- شهبازان (27) درصد، کواترنر (25) درصد، گچساران (20) درصد بیشترین لندفرم های کارست را دارند. کمترین محدوده با لندفرم های کارستی متعلق به سه سازند بختیاری (5/0) درصد، گورپی (2) درصد و آغاجاری (3) درصد است. شهرستان پلدختر که در حوضه رودخانه کشکان واقع شده است اشکال کارستی آن توسعه یافته و تنوع اشکال آن فراوان است. نتایج مدل کوبالیکوا و کیرچنر نشان داد سراب تنگ سیاب با 11/5 امتیاز بالاترین امتیاز را به دلائل ارزش علمی، آموزشی، اقتصادی و وضعیت دسترسی و زیرساخت های اولیه گردشگری، وجود ارزش های فرهنگی و زیست محیطی بدست آورد. بعد از آن نیز ژئوسایت های تنگه شیرز، تنگه هلت، چشمه شیرین ملاوی و غار پل خدا شیرز هر کدام با 10/5 امتیاز رتبه دوم، ژئوسایت-های غار کلماکره، چشمه سید سهل الدین، آبشار افرینه و دره خزینه هر کدام با 10 امتیاز رتبه سوم را به دلائل ارزش های علمی، آموزشی، اقتصادی و تنوع چشم انداز، نادر بودن در سطح منطقه، ملی، فراملی و وضعیت دسترسی و ارزش زیست-محیطی به خود اختصاص دادند.Evaluation of the geotourism capabilities of karst areas in the southwest of Lorestan province
The southwestern region of Lorestan is located in the folded Zagros region. In Iran, karst areas cover about 11% of the country's area, and most of these areas are located in the Zagros belt. Most of the lithological units of this study area have calcareous and soluble structure. For this reason, various karst geomorphosites have been formed in the southwest of Lorestan in two watersheds of Kashkan (Poldakhter and Mamolan counties) and Simre watershed (Kuhdasht and Rumeshkan counties). A large number of these geomorphosites can be considered tourist destinations. The purpose of this research is to evaluate the geotourism capabilities of karstic formations in the southwest of Lorestan province through the model of Kobalikova and Kirchner (2016). The statistical population of the research includes 8 experts of the Cultural Heritage Organization and 7 professors of Lorestan University. According to the obtained results, three formations, Asmari-Shahbazan (27%), Quaternary (25%), Gachsaran (20%), have the highest karst landforms. The results of Kubalikova and Kirchner's model showed that Sarab Teng Siab with 11.5 points got the highest score due to the scientific, educational, economic value and access status and basic infrastructure of tourism, the existence of cultural and environmental values. The geosites of Shirez Gorge, Helt Gorge, Cheshme Shirin Malawi and Ghar Pol Khoda Shirez each rank second with 10.5 points, the geosites of Ghar Kalmakre, Seyed Sahluddin Spring, Efreeneh Waterfall and Khazeena Valley each rank third with 10 points. due to the scientific, educational, economic values and landscape diversity, rarity at the regional, national, and international levels, and access status and environmental value. Gharali geosites of Gizan (5.3 points), Teng Gauzardeh (4.5 points) and Chep Kul Valley and Tulkesh Cheshme with 5 points are the least rated landforms in the southwest of Lorestan. The indicators of Kubalikova and Kirchner's model have not been able to attract tourists from scientific, educational, economic, conservation and cultural aspects.The southwestern region of Lorestan is located in the folded Zagros region. In Iran, karst areas cover about 11% of the country's area, and most of these areas are located in the Zagros belt. Most of the lithological units of this study area have calcareous and soluble structure. For this reason, various karst geomorphosites have been formed in the southwest of Lorestan in two watersheds of Kashkan (Poldakhter and Mamolan counties) and Simre watershed (Kuhdasht and Rumeshkan counties). A large number of these geomorphosites can be considered tourist destinations. The purpose of this research is to evaluate the geotourism capabilities of karstic formations in the southwest of Lorestan province through the model of Kobalikova and Kirchner (2016). The statistical population of the research includes 8 experts of the Cultural Heritage Organization and 7 professors of Lorestan University. According to the obtained results, three formations, Asmari-Shahbazan (27%), Quaternary (25%), Gachsaran (20%), have the highest karst landforms. The results of Kubalikova and Kirchner's model showed that Sarab Teng Siab with 11.5 points got the highest score due to the scientific, educational, economic value and access status and basic infrastructure of tourism, the existence of cultural and environmental values. The geosites of Shirez Gorge, Helt Gorge, Cheshme Shirin Malawi and Ghar Pol Khoda Shirez each rank second with 10.5 points, the geosites of Ghar Kalmakre, Seyed Sahluddin Spring, Efreeneh Waterfall and Khazeena Valley each rank third with 10 points. due to the scientific, educational, economic values and landscape diversity, rarity at the regional, national, and international levels, and access status and environmental value. Gharali geosites of Gizan (5.3 points), Teng Gauzardeh (4.5 points) and Chep Kul Valley and Tulkesh Cheshme with 5 points are the least rated landforms in the southwest of Lorestan. The indicators of Kubalikova and Kirchner's model have not been able to attract tourists from scientific, educational, economic, conservation and cultural aspects.The southwestern region of Lorestan is located in the folded Zagros region. In Iran, karst areas cover about 11% of the country's area, and most of these areas are located in the Zagros belt. Most of the lithological units of this study area have calcareous and soluble structure. For this reason, various karst geomorphosites have been formed in the southwest of Lorestan in two watersheds of Kashkan (Poldakhter and Mamolan counties) and Simre watershed (Kuhdasht and Rumeshkan counties). A large number of these geomorphosites can be considered tourist destinations. The purpose of this research is to evaluate the geotourism capabilities of karstic formations in the southwest of Lorestan province through the model of Kobalikova and Kirchner (2016). The statistical population of the research includes 8 experts of the Cultural Heritage Organization and 7 professors of Lorestan University. According to the obtained results, three formations, Asmari-Shahbazan (27%), Quaternary (25%), Gachsaran (20%), have the highest karst landforms. The results of Kubalikova and Kirchner's model showed that Sarab Teng Siab with 11.5 points got the highest score due to the scientific, educational, economic value and access status and basic infrastructure of tourism, the existence of cultural and environmental values. The geosites of Shirez Gorge, Helt Gorge, Cheshme Shirin Malawi and Ghar Pol Khoda Shirez each rank second with 10.5 points, the geosites of Ghar Kalmakre, Seyed Sahluddin Spring, Efreeneh Waterfall and Khazeena Valley each rank third with 10 points. due to the scientific, educational, economic values and landscape diversity, rarity at the regional, national, and international levels, and access status and environmental value. Gharali geosites of Gizan (5.3 points), Teng Gauzardeh (4.5 points) and Chep Kul Valley and Tulkesh Cheshme with 5 points are the least rated landforms in the southwest of Lorestan. The indicators of Kubalikova and Kirchner's model have not been able to attract tourists from scientific, educational, economic, conservation and cultural aspects.
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